Based on multi-beam bathymetric data and 2D high-resolution, multi-channel seismic prof＇des, combing ODPl148 drilling data, the morphology, internal sedimentary architecture, and evo-lution pattern of 17 deepwater ca...Based on multi-beam bathymetric data and 2D high-resolution, multi-channel seismic prof＇des, combing ODPl148 drilling data, the morphology, internal sedimentary architecture, and evo-lution pattern of 17 deepwater canyons from the Middle Miocene to present are documented in the northern Baiyun （白云） sag （BS）, Pearl River Mouth basin （PRMB）, and northern South China Sea （SCS）. There exist six seismic architectural elements in these canyons, including basal erosive surfaces （BES）, thalweg deposits （TD）, lateral migration packages （LMP）, mass transport deposits （MTD）, can- yon margin deposits （CMD）, and drape deposits （DD）. According to the stratigraphical ages and geo-metrical features of these canyons, their formation and evolution processes are divided into three stages： （1） Middle Miocene scouring-filling, （2） Late Miocene lateral migration, and （3） Pliocene-Quaternary vertical overlay. An auto-cyclic progressive process of eroding and filling by turbidity currents results in the scouring-filling and vertical overlay; bottom currents are responsible for the remarkable asym-metry between the two flanks of canyons; and faults are inherent dynamic forces triggering these can yons. It is inferred that these canyons are caused by the double effects of turbidity and bottom currents under the control of faults as inherent dynamic forces.展开更多
基金supported by the CAS Knowledge Innovation Program of China (No. KZCX2-YW-229)the National Natural Science Foundation of China (Nos. 40930845,2009CB219505)
文摘Based on multi-beam bathymetric data and 2D high-resolution, multi-channel seismic prof＇des, combing ODPl148 drilling data, the morphology, internal sedimentary architecture, and evo-lution pattern of 17 deepwater canyons from the Middle Miocene to present are documented in the northern Baiyun （白云） sag （BS）, Pearl River Mouth basin （PRMB）, and northern South China Sea （SCS）. There exist six seismic architectural elements in these canyons, including basal erosive surfaces （BES）, thalweg deposits （TD）, lateral migration packages （LMP）, mass transport deposits （MTD）, can- yon margin deposits （CMD）, and drape deposits （DD）. According to the stratigraphical ages and geo-metrical features of these canyons, their formation and evolution processes are divided into three stages： （1） Middle Miocene scouring-filling, （2） Late Miocene lateral migration, and （3） Pliocene-Quaternary vertical overlay. An auto-cyclic progressive process of eroding and filling by turbidity currents results in the scouring-filling and vertical overlay; bottom currents are responsible for the remarkable asym-metry between the two flanks of canyons; and faults are inherent dynamic forces triggering these can yons. It is inferred that these canyons are caused by the double effects of turbidity and bottom currents under the control of faults as inherent dynamic forces.
